M
Massimo Pompilio
Researcher at National Institute of Geophysics and Volcanology
Publications - 93
Citations - 4227
Massimo Pompilio is an academic researcher from National Institute of Geophysics and Volcanology. The author has contributed to research in topics: Volcano & Magma. The author has an hindex of 32, co-authored 87 publications receiving 3785 citations. Previous affiliations of Massimo Pompilio include University of Pisa & University of Catania.
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Journal ArticleDOI
Obliquity-paced Pliocene West Antarctic ice sheet oscillations
Tim R Naish,Tim R Naish,Ross D. Powell,Richard H. Levy,Richard H. Levy,Gary S. Wilson,Reed P. Scherer,Franco M Talarico,Lawrence A. Krissek,Frank Niessen,Massimo Pompilio,Terry J. Wilson,Lionel Carter,Robert M. DeConto,Peter Huybers,Robert M. McKay,David Pollard,James Ross,D. Winter,Peter Barrett,Greg H. Browne,Rosemary Cody,Rosemary Cody,Ellen A. Cowan,James S. Crampton,Gavin B. Dunbar,Nelia W. Dunbar,Fabio Florindo,Catalina Gebhardt,Ian J. Graham,M. J. Hannah,Dhiresh Hansaraj,Dhiresh Hansaraj,David M. Harwood,D. Helling,Stuart Henrys,Linda A. Hinnov,Gerhard Kuhn,Philip R. Kyle,Andreas Läufer,P. Maffioli,Diana Magens,Kevin W. Mandernack,William C. McIntosh,C. Millan,Roger H. Morin,Christian Ohneiser,Timothy Paulsen,Davide Persico,Ian Raine,J. Reed,J. Reed,Christina R. Riesselman,Leonardo Sagnotti,Douglas R. Schmitt,Charlotte Sjunneskog,P. Strong,Marco Taviani,S. W. Vogel,T. I. Wilch,Trevor Williams +60 more
TL;DR: A marine glacial record from the upper 600 m of the AND-1B sediment core recovered from beneath the northwest part of the Ross ice shelf is presented and well-dated, ∼40-kyr cyclic variations in ice-sheet extent linked to cycles in insolation influenced by changes in the Earth’s axial tilt (obliquity) during the Pliocene are demonstrated.
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A multi-disciplinary study of the 2002-03 Etna eruption: insights into a complex plumbing system
Daniele Andronico,Stefano Branca,Sonia Calvari,Mike Burton,Tommaso Caltabiano,Rosa Anna Corsaro,Paola Del Carlo,Gaetano Garfì,Luigi Lodato,Lusia Miraglia,Filippo Murè,Marco Neri,Emilio Pecora,Massimo Pompilio,G. Salerno,Letizia Spampinato +15 more
TL;DR: The 2002-03 Mt Etna flank eruption began on 26 October 2002 and finished on 28 January 2003, after three months of continuous explosive activity and discontinuous lava flow output.
Journal ArticleDOI
Conduit processes during the July-August 2001 explosive activity of Mt. Etna (Italy) : inferences from glass chemistry and crystal size distribution of ash particles
TL;DR: In this article, the authors investigated the causes of the transitions between style of basaltic explosion at Mt. Etna from July 19 to August 7, 2001, and provided a good case study to investigate the causes.
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Effects of magma storage and ascent on the kinetics of crystal growth
TL;DR: The size distributions of olivine, plagioclase and oxides of the 1991/93 eruption at Mt. Etna (Italy) were analyzed in this article, showing that the main features of the volcano feeding system have not changed despite observed variations in the magma output rates.
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Dynamic plumbing system beneath volcanoes revealed by kinetic modeling, and the connection to monitoring data: An example from Mt. Etna
TL;DR: In this article, the authors used the record preserved in compositional zoning of erupted minerals to reconstruct sections of the plumbing system of Mt. Etna (Sicily) during its 1991-1993 SE-flank eruption.